Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming

Methane seepage from continental slopes has been attributed to gas hydrate dissociation induced by anthropogenic bottom water warming. Here, the authors show that hydrates dissociated before the Anthropocene when the isostatic rebound induced by deglaciation of the Arctic ice sheet outpaced eustatic...

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Autores principales: Klaus Wallmann, M. Riedel, W. L. Hong, H. Patton, A. Hubbard, T. Pape, C. W. Hsu, C. Schmidt, J. E. Johnson, M. E. Torres, K. Andreassen, C. Berndt, G. Bohrmann
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Publicado: Nature Portfolio 2018
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Acceso en línea:https://doaj.org/article/530f09c916b24d5e929a4fbe52e5b05c
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spelling oai:doaj.org-article:530f09c916b24d5e929a4fbe52e5b05c2021-12-02T14:39:06ZGas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming10.1038/s41467-017-02550-92041-1723https://doaj.org/article/530f09c916b24d5e929a4fbe52e5b05c2018-01-01T00:00:00Zhttps://doi.org/10.1038/s41467-017-02550-9https://doaj.org/toc/2041-1723Methane seepage from continental slopes has been attributed to gas hydrate dissociation induced by anthropogenic bottom water warming. Here, the authors show that hydrates dissociated before the Anthropocene when the isostatic rebound induced by deglaciation of the Arctic ice sheet outpaced eustatic sea-level rise.Klaus WallmannM. RiedelW. L. HongH. PattonA. HubbardT. PapeC. W. HsuC. SchmidtJ. E. JohnsonM. E. TorresK. AndreassenC. BerndtG. BohrmannNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-9 (2018)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Klaus Wallmann
M. Riedel
W. L. Hong
H. Patton
A. Hubbard
T. Pape
C. W. Hsu
C. Schmidt
J. E. Johnson
M. E. Torres
K. Andreassen
C. Berndt
G. Bohrmann
Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming
description Methane seepage from continental slopes has been attributed to gas hydrate dissociation induced by anthropogenic bottom water warming. Here, the authors show that hydrates dissociated before the Anthropocene when the isostatic rebound induced by deglaciation of the Arctic ice sheet outpaced eustatic sea-level rise.
format article
author Klaus Wallmann
M. Riedel
W. L. Hong
H. Patton
A. Hubbard
T. Pape
C. W. Hsu
C. Schmidt
J. E. Johnson
M. E. Torres
K. Andreassen
C. Berndt
G. Bohrmann
author_facet Klaus Wallmann
M. Riedel
W. L. Hong
H. Patton
A. Hubbard
T. Pape
C. W. Hsu
C. Schmidt
J. E. Johnson
M. E. Torres
K. Andreassen
C. Berndt
G. Bohrmann
author_sort Klaus Wallmann
title Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming
title_short Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming
title_full Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming
title_fullStr Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming
title_full_unstemmed Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming
title_sort gas hydrate dissociation off svalbard induced by isostatic rebound rather than global warming
publisher Nature Portfolio
publishDate 2018
url https://doaj.org/article/530f09c916b24d5e929a4fbe52e5b05c
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